Kenbridge Project

The Kenbridge nickel deposit is hosted by an oval shaped gabbroic suite and has a distinct â€śbreccia pipeâ€ť appearance. Interpretation of outcrop lithological information is slightly complicated by deformation and metamorphism (regionally up to upper greenschist facies and with overprints of local contact metamorphism), and selective exposure within the project area. The following general rock descriptions have been modified from previous detailed outcrop mapping and reports (circa 1950â€™s).

Kenbridge Deposit

Three principal lineament trends are mapped and reflect both syn- and post- gabbro
intrusive events. Northeast-trending lineaments are the most prominent in the Kenbridge
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area and are reflected in the shearing and faulting of the rocks. The Kenbridge Deposit
coincides with the main northeast-trending deformation zone. North-, east-, and
northwest-trending lineaments are also common in the region. The east-trending
lineaments appear to control the larger mafic-ultramafic